Abstract Intraplate volcanism in Northeast Asia, located in a distant back‐arc setting, challenges conventional models of mantle convection and volatile cycling. Using receiver function data from over 300 broadband stations, we image the mantle transition zone (MTZ) beneath the Changbaishan/Paektu volcano.
Cunrui Han +6 more
wiley +1 more source
Tracing halogen and B cycling in subduction zones based on obducted, subducted and forearc serpentinites of the Dominican Republic. [PDF]
Pagé L, Hattori K.
europepmc +1 more source
Regional variability but global flux balance in the deep sulfur cycle. [PDF]
Li JL +6 more
europepmc +1 more source
Decoupling of high-pressure H2 production from serpentinization and magnetite in subduction zones
Siron G +4 more
europepmc +1 more source
Rheologic controls on the depth dependence of megathrust earthquakes. [PDF]
French ME, Delph JR, Condit CB.
europepmc +1 more source
How subduction evolution drives sediment-hosted mineralisation along craton edges. [PDF]
Shirmard H +4 more
europepmc +1 more source
Eastern Himalayan syntaxis formation controlled by slab flattening and crustal shear localization. [PDF]
van Agtmaal L +4 more
europepmc +1 more source
Ultralow-angle faults produce giant earthquakes. [PDF]
Ide S, Furuichi M, Sato DSK.
europepmc +1 more source
Integrated remote sensing and geochemical data of Shadli mineralized metavolcanics (Egypt): mantle plume-driven magmatism during subduction-rift transition. [PDF]
Khedr MZ +8 more
europepmc +1 more source

